What (the council members) want is what the Atlanta Police Foundation wants, which is to continue to militarize police and to attack our movements and criminalize our people. “The City Council has failed over and over again to listen to the masses of people in Atlanta. “The people need to have a voice in whether or not there is a Cop City,” community organizer Kamau Franklin said during a news conference. They would also have to raise hundreds of thousands of dollars to pay canvassers to help them do that. In order for the language to get on the ballot, though, organizers must first gather the signatures of more than 70,000 Atlanta voters over 60 days once the city clerk approves the petition. Under the proposed referendum, voters would choose whether they want to repeal the ordinance that authorized the lease of the city-owned land upon which the project is set to be built. Since hail can cause the rainfall estimates to be higher than what is actually occurring, steps are taken to prevent these high dBZ values from being converted to rainfall.ATLANTA (AP) - Activists announced an effort Wednesday to force a referendum that would allow Atlanta voters to decide whether the construction of a proposed police and firefighter training center should proceed, in a potential last-ditch effort to halt the project that its opponents refer to as “Cop City.”Ī day after the City Council rejected protesters’ pleas to refuse to fund the training facility, the activists returned to City Hall to file a referendum petition, hoping to take the fight to the ballot box. Hail is a good reflector of energy and will return very high dBZ values. These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time. Depending on the type of weather occurring and the area of the U.S., forecasters use a set of rainrates which are associated to the dBZ values. The higher the dBZ, the stronger the rainrate. Typically, light rain is occurring when the dBZ value reaches 20. The scale of dBZ values is also related to the intensity of rainfall. The value of the dBZ depends upon the mode the radar is in at the time the image was created. Notice the color on each scale remains the same in both operational modes, only the values change. The other scale (near left) represents dBZ values when the radar is in precipitation mode (dBZ values from 5 to 75). One scale (far left) represents dBZ values when the radar is in clear air mode (dBZ values from -28 to +28). Each reflectivity image you see includes one of two color scales. The dBZ values increase as the strength of the signal returned to the radar increases. So, a more convenient number for calculations and comparison, a decibel (or logarithmic) scale (dBZ), is used. Reflectivity (designated by the letter Z) covers a wide range of signals (from very weak to very strong). "Reflectivity" is the amount of transmitted power returned to the radar receiver. ![]() The colors are the different echo intensities (reflectivity) measured in dBZ (decibels of Z) during each elevation scan.
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